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- W2386951228 abstract "After mining over years,P3c aquifer groundwater formed an underground reservoir conducted by separated fissures and T1j aquifer groundwater formed an unified aquiferconducted by extensional fissures in Nantong coal mine.We conclude that aquifer destruction patterns are:mining destruction,destruction of sealed adverse borehole destruction of water conductive fault.The unified Aquiferin T1j and underground reservoirin P3c are favorable area for searching groundwater in hilly mining subsidence area in Southern China." @default.
- W2386951228 created "2016-06-24" @default.
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- W2386951228 date "2014-01-01" @default.
- W2386951228 modified "2023-09-26" @default.
- W2386951228 title "Study on favorable area for searching groundwater in Hilly mining subsidence Area in Southern China" @default.
- W2386951228 hasPublicationYear "2014" @default.
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